Isotopic Composition of Abiogenic Gas Produced in Closed-System Fischer-Tropsch Synthesis: Implications for the Origins of the Deep Songliao Basin Gases in China

<div>Carbon isotope fractionation under different conditions (data from [<a href="/journals/geofluids/2019/2823803/#B21">21</a>, <a href="/journals/geofluids/2019/2823803/#B69">69</a>, <a href="/journals/geofluids/2019/2823803/#B71">71</a>, <a href="/journals/geofluids/2019/2823803/#B72">72</a>]; Proskurowski et al. 2008; [<a href="/journals/geofluids/2019/2823803/#B84">84</a>, <a href="/journals/geofluids/2019/2823803/#B85">85</a>]).</div>

Geofluids

fig7

Figure 7

Figure 7: Isotopic Composition of Abiogenic Gas Produced in Closed-System Fischer-Tropsch Synthesis: Implications for the Origins of the Deep Songliao Basin Gases in China 

Figure 7 | Isotopic Composition of Abiogenic Gas Produced in Closed-System Fischer-Tropsch Synthesis: Implications for the Origins of the Deep Songliao Basin Gases in China 